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  • Other Sources  (3)
  • Cambridge University Press  (2)
  • AAPG (American Association of Petroleum Geologists)  (1)
  • 1990-1994
  • 1980-1984
  • 1960-1964  (3)
  • 1962  (3)
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  • 1990-1994
  • 1980-1984
  • 1960-1964  (3)
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  • 1
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    Cambridge University Press
    In:  Geological Magazine, 99 (02). pp. 164-172.
    Publication Date: 2020-07-31
    Description: The results of an examination of one quarry within the gneisses of the Bartica Assemblage are described and the validity of these results throughout the whole of the Bartica Assemblage is discussed. The foliation and banding of the gneisses at Kereti Quarry are mainly the results of tectonism; concomitant metamorphism within the Amphibolite Facies was succeeded by a two-phase metasomatism involving successive additions of Na and K. These results appear valid throughout the Bartica Assemblage and it is further suggested that the main rock type distribution in the Bartica Assemblage is also controlled by tectonism.
    Type: Article , PeerReviewed
    Format: text
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  • 2
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    Cambridge University Press
    In:  Journal of Fluid Mechanics, 12 (04). p. 481.
    Publication Date: 2020-07-24
    Description: The energy flux in a finite-depth gravity-wave spectrum resulting from weak non-linear couplings between the spectral components is evaluated by means of a perturbation method. The fifth-order analysis yields a fourth-order effect comparable in magnitude to the generating and dissipating processes in wind-generated seas. The energy flux favours equidistribution of energy and vanishes in the limiting case of a white, isotropic spectrum. The influence on the equilibrium structure of fully developed wave spectra and on other phenomena in random seas is discussed briefly.
    Type: Article , PeerReviewed
    Format: text
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  • 3
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    AAPG (American Association of Petroleum Geologists)
    In:  In: Classification of Carbonate Rocks — A Symposium. , ed. by Ham , W. E. AAPG Memoir, 1 . AAPG (American Association of Petroleum Geologists), Tulsa, Oklahoma, pp. 108-121. ISBN 9781629812366
    Publication Date: 2021-01-27
    Description: Three textural features seem especially useful in classifying those carbonate rocks that retain their depositional texture (1) Presence or absence of carbonate mud, which differentiates muddy carbonate from grainstone; (2) abundance of grains, which allows muddy carbonates to be subdivided into mudstone, wackestone, and packstone; and (3) presence of signs of binding during deposition, which characterizes boundstone. The distinction between grain-support and mud-support differentiates packstone from wackestone—packstone is full of its particular mixture of grains, wackestone is not. Rocks retaining too little of their depositional texture to be classified are set aside as crystalline carbonates.
    Type: Book chapter , NonPeerReviewed
    Format: text
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